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Ragna Mine, Plenty River area, Huckitta Station, Central Desert Region, Northern Territory, Australiai
Regional Level Types
Ragna MineMine
Plenty River areaArea
Huckitta Station- not defined -
Central Desert RegionRegion
Northern TerritoryTerritory
AustraliaCountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
22° 51' 22'' South , 135° 32' 5'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
295287
Long-form identifier:
mindat:1:2:295287:4
GUID (UUID V4):
f61490f6-bd97-4077-98ec-16ef6aea820d


A former mica mine.

Located approximately 5 kilometres north-east of the Huckitta pastoral station homestead. Satellite images indicate several scattered small workings across a flat area. None are directly accessed by a track, the nearest being the track which passes the Whistleduck Mine to the south.

Rochow describes the old and new workings, but it is unclear which of the small workings seen relate to this. Mindat map denotes roughly the centre of the widely scattered workings.

The old workings contain an open cut, 40 by 15 by 12 feet deep, on a fine grained pegmatite containing quartz, potash feldspar, beryl, and ruby mica. A second site is noted containing two pits, 5 feet across, and 3-5 feet deep on a coarse grained pegmatite. A third site contains on open cut 60 feet long, 5-10 feet wide, and 6-10 feet deep, on a fine to medium grained pegmatite, dipping 65 degrees east, with an irregular footwall vein, 5-10 feet thick, and no zoning.

No mention is made on the history of the new workings, but it is assumed based on the history of the field, these relate to the 1950's. One site contains 2 pits in a mica rich quartz pegmatite pipe marginal zone. The quartz core of the pegmatite is 6 feet thick. Another site contains an open cut 44 feet long, and 15 feet deep, following the hanging wall on a medium grained pegmatite, to a maximum of 6 feet thick, dipping 65 degrees west, with no quartz core. A third site contains a 12 foot deep shaft on a schorl rich pegmatite pipe, 4-5 feet thick, the feldspar partly kaolinised. Lastly a fourth pit is noted, irregular in shape, 8 feet deep, on a complex pegmatite/gneiss mixture. The pegmatite forms small lenses up to 2 feet thick in bands of gneiss also 2 feet thick.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


4 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 9 - Silicates
Beryl9.CJ.05Be3Al2(Si6O18)
Schorl9.CK.05NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
Kaolinite9.ED.05Al2(Si2O5)(OH)4
Unclassified
'Feldspar Group'-
'Mica Group'-

List of minerals for each chemical element

HHydrogen
H KaoliniteAl2(Si2O5)(OH)4
H SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
BeBeryllium
Be BerylBe3Al2(Si6O18)
BBoron
B SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
OOxygen
O BerylBe3Al2(Si6O18)
O KaoliniteAl2(Si2O5)(OH)4
O QuartzSiO2
O SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
NaSodium
Na SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
AlAluminium
Al BerylBe3Al2(Si6O18)
Al KaoliniteAl2(Si2O5)(OH)4
Al SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
SiSilicon
Si BerylBe3Al2(Si6O18)
Si KaoliniteAl2(Si2O5)(OH)4
Si QuartzSiO2
Si SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
FeIron
Fe SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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